EGU23-16507
https://doi.org/10.5194/egusphere-egu23-16507
EGU General Assembly 2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.

Drawbacks in modeling debris flow erosion using the shallow water equations and the finite volume method. Examples from FLATModel and the Rebaixader torrent

Vicente Medina, Marcel Hürlimann, and Laura Molano
Vicente Medina et al.
  • Division of Geotechnical Engineering and Geosciences; Department of Civil and Environmental Engineering, UPC BarcelonaTECH; 08034 Barcelona, Spain (vicente.de.medina@upc.edu)

FLATModel (Medina et al. 2008) was developed as a modeling tool for debris flow (DF) events. It includes several specific DF features, among them, a simple erosion mechanism was proposed and implemented. The previous validation of this model capability was based on event volume comparison. Now, a more detailed analysis has been performed, and several constraints in its applicability emerge. Model results for erosion present an important dependence on numerical parameters configuration, hence, not only the physical parameters calibration is required. Accuracy in erosion modeling requires proper numeric setup resulting in high computational effort, compromising the model performance. New specific algorithm or erosion computation approach is required.
A part from these numerical aspects, we present some results obtained in the Rebaixader torrent (Central Pyrenees), where a debris-flow monitoring system is installed and annual UAV-surveys are performed.


Medina, V., Hürlimann, M., Bateman, A. (2008) FLATModel: 2D finite volume code for debris-flow modelling. Application to different events occurred in the Northeastern part of the Iberian Peninsula. Landslides, 5, 127-142. https://doi.org/10.1007/s10346-007-0102-3

How to cite: Medina, V., Hürlimann, M., and Molano, L.: Drawbacks in modeling debris flow erosion using the shallow water equations and the finite volume method. Examples from FLATModel and the Rebaixader torrent, EGU General Assembly 2023, Vienna, Austria, 24–28 Apr 2023, EGU23-16507, https://doi.org/10.5194/egusphere-egu23-16507, 2023.